Time and Metamorphic Petrology: Calcite to Aragonite Experiments
Although the equilibrium phase relations of many mineral systems are generally well established, the rates of transformations, particularly in polycrystalline rocks, are not. The results of experiments on the calcite to aragonite transformation in polycrystalline marble are different from those for...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 1992-10, Vol.258 (5079), p.110-112 |
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